首页> 外文期刊>Journal of geophysical research. Solid earth: JGR >Probabilistic seismic hazard in the San Francisco Bay area based on a simplified viscoelastic cycle model of fault interactions
【24h】

Probabilistic seismic hazard in the San Francisco Bay area based on a simplified viscoelastic cycle model of fault interactions

机译:基于简化的断层相互作用的粘弹性循环模型的旧金山湾地区概率地震危险性

获取原文
获取原文并翻译 | 示例
       

摘要

We construct a viscoelastic cycle model of plate boundary deformation that includes the effect of time-dependent interseismic strain accumulation, coseismic strain release, and viscoelastic relaxation of the substrate beneath the seismogenic crust. For a given fault system, time-averaged stress changes at any point (not on a fault) are constrained to zero; that is, kinematic consistency is enforced for the fault system. The dates of last rupture, mean recurrence times, and the slip distributions of the (assumed) repeating ruptures are key inputs into the viscoelastic cycle model. This simple formulation allows construction of stress evolution at all points in the plate boundary zone for purposes of probabilistic seismic hazard analysis (PSHA). Stress evolution is combined with a Coulomb failure stress threshold at representative points on the fault segments to estimate the times of their respective future ruptures. In our PSHA we consider uncertainties in a four-dimensional parameter space: the rupture peridocities, slip distributions, time of last earthquake (for prehistoric ruptures) and Coulomb failure stress thresholds. We apply this methodology to the San Francisco Bay region using a recently determined fault chronology of area faults. Assuming single-segment rupture scenarios, we find that future rupture probabilities of area faults in the coming decades are the highest for the southern Hayward, Rodgers Creek, and northern Calaveras faults. This conclusion is qualitatively similar to that of Working Group on California Earthquake Probabilities, but the probabilities derived here are significantly higher. Given that fault rupture probabilities are highly model-dependent, no single model should be used to assess to time-dependent rupture probabilities. We suggest that several models, including the present one, be used in a comprehensive PSHA methodology, as was done by Working Group on California Earthquake Probabilities.
机译:我们构造了板块边界变形的粘弹性循环模型,该模型包括随时间变化的间震应变累积,同震应变释放以及震源壳下方基底的粘弹性松弛的影响。对于给定的故障系统,在任意点(不在故障上)的时间平均应力变化被约束为零;就是说,对于故障系统而言,运动学上的一致性是必须的。上次破裂的日期,平均复发时间和(假定的)重复破裂的滑动分布是粘弹性循环模型的关键输入。这种简单的公式允许在板边界区域的所有点构造应力演化,以进行概率地震危险性分析(PSHA)。在断层段的代表性点上,将应力演化与库仑破坏应力阈值结合起来,以估计它们各自未来破裂的时间。在我们的PSHA中,我们考虑了一个二维参数空间中的不确定性:破裂围岩,滑动分布,上次地震的时间(对于史前破裂)和库仑破坏应力阈值。我们使用最近确定的区域断层年代学将此方法应用于旧金山湾地区。假设单段破裂情景,我们发现未来几十年区域断层的破裂概率是南部海沃德,罗杰斯溪和卡拉维拉斯北部断层的最高破裂概率。该结论在质量上与加利福尼亚地震概率工作组的结论相似,但此处得出的概率要高得多。鉴于断层破裂概率高度依赖于模型,因此不应使用单个模型来评估随时间变化的破裂概率。我们建议像加利福尼亚地震概率工作组所做的那样,在综合的PSHA方法中使用几种模型,包括当前的模型。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号